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Experimental study on selective adsorption/desorption of CO and CH behavior on shale under high pressure condition 2
4
Zihao Yang, Zhaoxia Dong, Liu Wang, Taiheng Yin, Xinyu Fan, Meiqin Lin, and Juan Zhang Energy Fuels, Just Accepted Manuscript • DOI: 10.1021/acs.energyfuels.8b02068 • Publication Date (Web): 07 Aug 2018 Downloaded from http://pubs.acs.org on August 8, 2018
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Experimental study on selective adsorption/desorption of CO2 and CH4 behavior on shale under high pressure condition
5
Zihao Yang,* Zhaoxia Dong, Liu Wang, Taiheng Yin, Xinyu Fan, Meiqin Lin and
6
Juan Zhang
1 2 3
7
Institute of Enhanced Oil Recovery, China University of Petroleum (Beijing), Fuxue
8
Road 18, Changping, Beijing, 102249, China.
9
Abstract: The mechanisms of CO2 enhancing coal bed methane (ECBM) are
10
investigated by many works. The competitive adsorption of CO2 and methane on coal
11
is believed to be the dominant effect. However, whether CO2 injection can be used for
12
improving shale gas recovery is not well answered yet. The adsorption and desorption
13
behaviour of CO2, methane or their mixture on shale is seldom reported. To evaluate
14
the feasibility of the utilization of CO2 for enhancing shale gas recovery, adsorption
15
and desorption experiments of methane, carbon dioxide, and mixtures of the two
16
gases on shales from Qaidam basin have been operated by manometric method at
17
50 °C and pressures up to 5.0 MPa. The results show that for single component of
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CO2 or methane, preferential adsorption of CO2 on shale is observed. Meanwhile, the
19
adsorption behavior of mixtures of the two gases manifests that CH4 is preferentially
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adsorbed on shale instead of CO2, which means that during the adsorption process, the
21
existence of CO2 promoted the sorption of CH4. For the process of desorption, an
1
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opposite phenomenon is obtained, it is presented that with the pressure decreasing,
2
CO2 shows a higher adsorption ability on shale. During this period, the existence of
3
CO2 facilitates desorption of CH4, which may result in a higher recovery of shale gas.
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Based on the competitive adsorption experimental results, the utilization of CO2 to
5
improve shale gas recovery is practicable theoretically.
6 7
KEYWORDS: Shale Gas; Carbon Dioxide; Competitive Adsorption; Desorption
8 9
1. Introduction
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As an unconventional natural gas reservoir, shale gas has achieved huge success
11
in the exploration and development in the United States in recent years, which is
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greatly benefited from the advancements of horizontal drilling and hydrofracture
13
technologies.1 However, some issues caused by these technologies, such as excessive
14
consumption of water, leakage of shale gas, environmental pollution and treatment of
15
waste water, are emerging. Meanwhile, for shale reservoirs with strong water
16
sensitivity, the efficiency of such technologies will be reduced. Therefore,
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environmental friendly alternative technologies for shale gas recovery attract people's
18
attention.
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Under the double pressure of energy shortages and increasingly severe natural
20
disasters and social harm caused by the emission of greenhouse gases, the utilization
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of CO2 for exploring oil and gas can bring both environmental and economic
22
benefit.2,3 Many works has been done to investigate the feasibility and mechanisms of 2
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CO2 enhancing coal bed methane (ECBM).4-9 The preferential adsorption of CO2 on
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coal
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displacing the coalbed methane by CO2 injection; on the other hand,the reduction of
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the partial pressure of CH4 and the effect of repressurizing the coal reservoir by gas
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can both accelerate desorption of methane from the coalbed.10-12
is
demonstrated
to
be
the
most
important
mechanism
of
6
As reported, shale gas has the similar occurrence mechanism to that of coal bed
7
methane,13 meanwhile researchers have already studied the adsorption behavior of
8
single component of CO2 and CH4 on shale. During the process of adsorption, all the
9
studies have come to the unanimous conclusion that, adsorption capacity of CO2 on
10
shale is significantly higher than CH4, which is to say that CO2 has the ability to
11
displace the adsorbed CH4 from the shale surface in porous media.14-22 This result is
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also considered to be one of the important theoretical premises for the application of
13
CO2 to enhance gas recovery (CO2-EGR). Consequently, the utilization of injecting
14
CO2 is hopefully an alternative technology of enhancing shale gas recovery instead of
15
horizontal drilling or hydrofracture technology. Moreover, the previous work have
16
also provided the details of sample preparation,22 pre-treatment and the method of
17
adsorption experiment, which has referential value for further study.
18
However, for CO2-EGR, the practical situation is that CO2 and CH4 are mixed in
19
the reservoirs. Thus the adsorption behavior of the mixture is of significant
20
importance. The result will provide assertive evidence for whether CO2-EGR is
21
practicable for shale gas. Unfortunately, most previous researches focused on the
22
pure component adsorption on shale, there is almost no literature reporting the result 3
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of sorption behavior of the mixture on shale. The basic data of this field is devoid. To
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enrich the research in this field, study on the adsorption behavior of CH4 + CO2
3
system is of great importance. According to the literatures,23-26 the experimental
4
method of mixture gas sorption behaviors on coal is well established and can be used
5
for this study. Meanwhile, based on the experimental data, the adsorption rule of CH4
6
+ CO2 binary system on coal presents complex characteristic which is different with
7
single component adsorption. For the adsorption process on different coal, which
8
kind of gases was preferential adsorbed was not assured, and the adsorption
9
mechanism of binary system was not well investigated yet. Therefore, for the
10
adsorption and desorption process, only studying the single gas sorption is
11
insufficient, the research on the binary mixture system of CH4 and CO2 is imperative.
12
In this work, isothermal adsorption experiment was operated to investigate the
13
adsorption and desorption behavior of CO2, CH4 and their mixtures on shale. The law
14
of adsorption of these systems on shale was illuminated. According to the
15
competitive adsorption experimental results, the utilization of CO2 to improve shale
16
gas recovery is practicable theoretically.
17
2. Experimental section
18
2.1. Physical properties of shale
19
The shale used in this work was obtained from Qaidam basin. The pyrolysis
20
parameter was analyzed by Rock-Eval technology developed by France Petroleum
21
Research Institute. For conducting the pyrolysis analysis, the shale samples were
22
pulverized to 100-200 mesh powder. The details introductions of Rock-Eval can be 4
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found in the published literatures
. The pyrolysis analysis process was briefly
2
described as follows. The shale sample was first heated at 300 oC for 3 minutes in an
3
inert atmosphere. Then, a ramped heating stage of 25 oC/min was conducted until the
4
temperature reached 650 oC and kept the temperature constant for 1 min. Followed,
5
the sample was transferred into an oxic chamber where it is heated to 850 ºC, burning
6
off all the remaining organic-matter. The shale sample pyrolysis analysis result was
7
shown in Table 1. The result shows that the total organic carbon (TOC) of the shale
8
sample is 4.86%.
9
Table 1. Results of Rock pyrolysis analysis
10 TOC(%)
Tmax(℃)
S1(mg/g)
S2(mg/g)
S3(mg/g)
S4(mg/g)
4.86
433
2.13
28.47
0.89
23.25
11 12
The mineral composition of the shale was analyzed by X-Ray Diffraction (XRD)
13
and the result is listed in Table 2. It can be seen that the content of
14
brittle minerals such as quartz and feldspar is up to 40.1%, which is a relative higher
15
level. This data suggests that the shale sample is easily to be fractured. Meanwhile,
16
the content of clay is over 55%. As reported,30 clay minerals are an important
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adsorptive support for gases as well as organic matter, therefore the relative higher
18
content of clay bring benefits for shale gas adsorption.
19 20
Table 2. Analysis results of minerals in total shale rock 5
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Potash Composition
Quartz
Plagioclase
Calcite
Siderite
Clay
5.6
1.0
3.0
55.9
feldspar content 32.2
2.3
(wt%) 1 2
According to Kang’s reasearch,14 the pores are mainly existing in the organic
3
matter and the most of them are nanoscale micropore or mesopore. The method of
4
low-pressure nitrogen adsorption is adopted to analyze the pore structure of shale.31-33
5
The apparatus is ASAP 2460 surface area and porosity analyzer provided by
6
Micromeritics Instrument CORP, America.
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The shale samples with a particle size of < 0.113 mm are most suitable for
8
low-pressure nitrogen adsorption experiments.34 Therefore, for conducting the
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low-pressure nitrogen adsorption experiments the samples were crushed to 120-230
10
mesh size grains. Before analysis with either N2, the shale samples were automatically
11
degassed by heating at ∼110 °C in a vacuum for about 24 h. The low-pressure N2
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adsorption isotherms were measured over the relative equilibrium adsorption pressure
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(P/Po) ranges of 0.005–0.995 at 77.4 K. The pore volume, surface area, and pore size
14
distribution (PSD) could be calculated based on the N2 adsorption data using the
15
density functional theory method (DFT).34,35,36 The low-pressure nitrogen adsorption
16
experiments result is shown in Figure 1 and Table 3. In terms of the adsorption
17
isotherm category by International Union of Pure and Applied Chemistry (IUPAC), it
18
can be seen from Figure 1, the N2 adsorption curve on shale is similar with type Ⅳ, 6
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which indicates that mesopore is dominant. Simultaneously, single peak appears
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obviously at 3nm, which suggests that pore size is mainly nanoscale. As shown in
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Table 3, the specific surface area of the sample is 23.588 m2/g, which is much higher
4
than that of tight sandstone.37 This relative higher surface area can bring advantages
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for gas sorption. It also can be seen that the mesopore provides main contribution to
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specific surface area. Pore Width (nm) 0
20
40
60
80
3.5
3
Quantity Adsorbed (cm /g)
4.0
0.0010
3
dV/dw (cm /g.nm)
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0.0005
3.0 2.5
0.0000
2.0 1.5 1.0
Adsorption Desorption
0.5 0.0
0.0
0.2
0.4
0.8
1.0
Relative Pressure(P/P0)
7 8
0.6
Figure 1. Nitrogen adsorption and desorption isotherms and Pore size distributions
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Table 3. Nitrogen surface areas and pore volume
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Parameter
Pore types
Percentage(%)
Micropore Mesopore Macropore
Total
Micropore Mesopore Macropore
Specific surface 3.990
19.572
0.019
23.588
2
area(m /g)
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83.0
0.1
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Pore volume 0.005167
0.047828
0.00037
0.053365
9.7
89.6
(cm3 /g) 1
2.2. Experimental set-up
2
Shale samples were pulverized and sieved to obtain 120-230 mesh powder, and
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dried in the oven for over 48 h at 105 °C to remove moisture maintained in rock
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samples, and then sealed for future experiments. CO2 and CH4 with a purity of 99.9 %
5
are purchased from Beijing AP Beifen Gases Industry Company.
6
Based on the references which reported shale gas adsorption and desorption
7
experiments,22,24,38,39 we built up a device to study the single and multi-component
8
gases adsorption-desorption experiment adopting the experiment method which was
9
well introduced in the literatures. The schematic diagram is shown in Figure 2. For
10
adsorption and desorption behavior measurement, the main part apparatus mainly
11
consists of a sorption cell, a reference cell, and a series of valves and pipelines. The
12
main part is placed in the air bath oven under 50 °C. The temperature can be
13
controlled constant within ±0.15 °C of the set point. A pressure sensor with precision
14
of 0.05% is equipped (Max 25 MPa) and connected to the computer to record the
15
pressure variation of the system. For obtaining the accurate data of adsorption and
16
desorption, besides recording the pressure and temperature, the composition of the
17
equilibrium gas is also required to be analyzed by gas chromatography. To avoid the
18
error caused by the pressure variation during gas sampling process, a sampling cell is
19
designed as void volume. During the adsorption experiment, the sampling cell is
20
connected with adsorption cell, under the action of diffusion, the gas composition of 8
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the both cells are coincident with each other. When the adsorption equilibrium was
2
established, the valve between adsorption cell and sampling cell was closed and then
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the equilibrium gas was collected for further composition analysis. Leak test was
4
operated before each experiment. Helium was injected until the pressure reaching 12
5
MPa. The system was kept in the oven under 50 °C for 24 hours. If the leakage rate of
6
each cell is lower than 6.89×10-4 MPa/h, the system is considered with
7
excellent air-tightness.38
8
To obtain accurate data, it is necessary to calibrate the volume of the reference
9
cell (VRC), adsorption cell (VAC) and sampling cell (VSC). The void volume of the pines,
10
pressure sensor and six-way valve was included as a part of the volume of reference
11
cell. The blank volumes of the cells are measured by helium expansion. The mass
12
conservation equations of helium were established to calculate the volume. The
13
densities of helium under different pressures were calculated by Aspen Plus.(VRC
14
=54.077 cm3、VAC =170.010 cm3、VSC =9.193 cm3). After calibrating, a certain amount
15
of shale particles were packed in the adsorption cell and then the residual volume (Vd)
16
was measured by the method similar with the calibrating method.
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2.3. Adsorption and desorption experiments
18
For single gas adsorption and desorption measurement, after the process of
19
set-up, the system was vacuumed and adsorption experiment was operated. Based on
20
the previous result, adsorption equilibrium is considered to be achieved when the
21
pressure variation was less than 6.89×10-4 MPa/h.38 The pressure was increased step
22
by step up to 5MPa after each equilibrium being established. When the adsorption 9
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experiment was accomplished, the valve between adsorption cell and six-way was
2
closed. A certain amount of gas was released from reference cell and sampling cell
3
through needle valve, then the needle valve was closed and the pressure of a new
4
equilibrium was recorded. Next, the valve between adsorption cell and six-way was
5
opened and the pressure was recorded after adsorption equilibrium was obtained. To
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avoid air diffusing into the system, a one-way flow valve was connected at the outlet
7
end of the needle valve. The procedure restarts until the pressure minimum is reached.
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The amount of gas during adsorption or desorption period was calculated by mass
9
conservation. For the adsorption and desorption of mixture of CO2 and CH4, the
10
composition of equilibrium gases was analyzed by gas chromatograph. Different with
11
pure component adsorption process, the gas composition maybe changed after
12
adsorption equilibrium being achieved, thus the whole system needs to be vacuumed
13
after each experiment.
14 15
Figure 2. Schematic diagram of isothermal adsorption and desorption apparatus
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3. Results and discussion
17
3.1. Isothermal adsorption and desorption curve of CH4 and CO2
18
The isothermal adsorption and desorption curves of CH4 and CO2 on shale 10
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samples under different pressures up to 5 MPa at 50 °C are shown in Figure 3. 0.30
CH4 Adsorption CH4 Desorption CO2 Adsorption CO2 Desorption
0.25
Excess Adsorption (mmol/g)
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
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0.20
0.15
0.10
0.05
0.00 0
2
1000
2000
3000
4000
5000
Pressure (kPa)
3
Figure 3. CH4 and CO2 adsorption and desorption isotherms
4
It can be seen from Figure 3 that with the pressure being increased, the
5
adsorption amount of both CO2 and CH4 is aggrandized. Under the same condition of
6
pressure, the adsorption amount of CO2 on shale is significantly higher than that of
7
CH4. The hysteresis phenomenon is presented during the desorption procedure and for
8
CO2 gas the hysteresis phenomenon is more obvious than that of CH4 which implies
9
that the interaction between CO2 and shale is more stronger than that between CH4
10
and shale. Based on this result, it can be concluded that the adsorption ability of CO2
11
on shale is much higher than that of CH4, which is identical with the mechanisms of
12
CO2 enhancing coal bed methane (ECBM) and it can be tentatively considered that
13
the utilization of CO2 for enhancing shale gas is feasible. However, the subsequent
14
experiments are needed to furtherly prove this conclusion.
15
3.2. Isothermal adsorption and desorption of premixed gases
16
For the practical situation, there is already free shale gas existing in the reservoir, 11
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the actual selective adsorption behavior involves mixtures of CO2 and CH4.
2
Therefore, it is necessary to study the sorption property of mixture gas to investigate
3
whether CO2 can be utilized for shale gas recovery. In this work, 41.9%CO2 +
4
58.1%CH4 was prepared as mixture gas to study competitive adsorption.
5
During the adsorption process, if the competitive adsorption phenomenon of CO2
6
and CH4 on shale occurs, the composition of mixture gases should be changed. In the
7
adsorbed phase, the content of more preferential gas will be higher than that of the
8
feed gas. This is to say that the content of more preferential gas in free phase (gas
9
phase of adsorption equilibrium) will be lower than that in feed gas. The gas
10
composition of feed gas and free phase was analyzed by gas chromatograph. The
11
result is shown in Figure 4. From Figure 4, it can be seen that under the experimental
12
pressures, the fraction of CO2 of both feed gas and free gas are almost coincident. This
13
phenomenon indicates that for mixture system, CO2 does not present more
14
preferential adsorption ability on shale than CH4, which is an opposite result with pure
15
gas adsorption.
16
In the classical theory, it is stated that the adsorption energy of CO2 is higher than
17
CH4. When the pressure decreases, CH4 is desorbed preferentially, consequently the
18
fraction of CH4 in free phase will increase which results in that the content of CO2
19
decreases. With the desorption processing, the desorption rate of CH4 decreases and
20
meanwhile the desorption rate of CO2 increases. As a result, from the desorption
21
curve it can be seen that the fraction of CO2 in gas phase firstly decreases and then
22
increases as pressure decreasing which matches the classical theory. But for all the 12
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pressures conditions, CO2 concentration in free phase of desorption process is lower
2
than that in gas phase of adsorption process. In contrast, it can be inferred that the
3
fraction of CH4 in free phase during desorption is almost higher than that of
4
adsorption process. 0.46
Feed Adsorption Desorption
0.44
CO2 molar fraction
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0.42 0.40 0.38 0.36 0.34 0
1000
2000
3000
4000
5000
Pressure (kPa)
5 6 7
Figure 4. CO2 molar fraction of the feed gas and equilibrium composition of adsorption and desorption gas as a function of pressure.
8
To further realize the adsorption law of each component in mixture gas, the total
9
adsorption quantity of mixture gas was calculated according to pressure variation and
10
the adsorption capacity of CO2 and CH4 of mixture system was also calculated. The
11
result is shown in Figure 5. For comparison, the adsorption quantity of pure gas was
12
presented as well. It can be seen from Figure 5 that the adsorption capacity of each
13
gas increases with pressure. Because the different adsorption ability of CO2 and CH4,
14
the phenomenon of competitive adsorption on specific adsorption site occurs, as a
15
result under the same pressure the adsorption capacity of mixture gas is between that
16
of pure CO2 and CH4.39 Meanwhile, it can be seen that for mixture gas system, the 13
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adsorption capacity of CH4 is higher than that of CO2. This result proves that during
2
mixture gas adsorption process, CH4 shows higher adsorption ability which is
3
opposite with pure gas adsorption. It is also noted that the CH4 adsorption capacity of
4
mixture gas is even a bit higher than that of pure CH4 under the same pressure, which
5
implies that in this case the existence of CO2 in the mixture gas promotes CH4
6
adsorption. 0.30
Pure CH4 Pure CO2 Mixture CH4 (Mixture) CO2 (Mixture)
0.25
Excess Adsorption (mmol/g)
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
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0.20
0.15
0.10
0.05
0.00 0
7
8
1000
2000
3000
4000
5000
Pressure (kPa)
Figure 5. Pure CH4 and CO2,and their mixture adsorption isotherms.
9
For a binary system, the adsorption capacity of a component in mixture gas is
10
depending on the partial pressure. If one of the component cannot be adsorbed or its
11
adsorption capacity can be neglected (for example binary system of CH4 and He), the
12
adsorption capacity of the other component should be coincided with that of its pure
13
gas under the same condition of pressure.10 For the condition of that both the
14
components can be adsorbed (for example binary system of CH4 and CO2), due to
15
competitive adsorption, the adsorption capacity of each component is different with
16
its pure component. To investigate the interaction of CH4 and CO2 during adsorption 14
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period, the adsorption capacity as a function of gas partial pressure is shown in Figure
2
6 and Figure 7. 0.09
Pure CH4 CH4 (Mixture) CH4 Patial Pressure
0.08
Excess Adsorption (mmol/g)
0.07 0.06 0.05 0.04 0.03 0.02 0.01 0
1000
2000
3 4
3000
4000
5000
Pressure (kPa)
Figure 6. CH4 adsorption isotherm as a function of CH4 partial pressure.
5 0.28
Pure CO2 Mixture (CO2) CO2 Patial Pressure
0.26 0.24
Excess Adsorption (mmol/g)
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
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0.22 0.20 0.18 0.16 0.14 0.12 0.10 0.08 0.06 0.04 0.02 0
6 7
1000
2000
3000
4000
5000
Pressure (kPa)
Figure 7. CO2 adsorption isotherm as a function of CO2 partial pressure.
8
From Figure 6 it can be seen that the adsorption capacity of CH4 in mixture gas
9
is obviously higher than that of the same CH4 partial pressure. This result further
10
proves that the existence of CO2 does not block CH4 to be adsorbed but promotes the 15
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adsorption of CH4. This is to say, for binary gas system of CO2 and CH4, CH4 shows
2
advantage to be absorbed on shale. The same adsorption phenomenon of mixture gas
3
of CO2 and CH4 on low coal rank coal sample was also reported by Dai.40 Their
4
research also showed that the adsorption capacity of CH4 was affected by CO2 content
5
in the binary system.
6
Moreover, it can be seen from Figure 7 that the adsorption capacity of CO2 in
7
mixture gas is lower than that of the same CO2 partial pressure. When CO2 being
8
mixed with CH4, it can be concluded that CH4 molecules occupied adsorption site
9
preferentially which prevent subsequent CO2 adsorption. Therefore, according to
10
these result it seems that since there is already free CH4 in the shale gas reservoir,
11
injection of CO2 will facilitate CH4 adsorption and CO2 injection cannot be utilized
12
for shale gas recovery.
13
However, it should be noticed that the exploitation procedure of shale gas is
14
mainly depending on pressure deceasing process which means we should focus on the
15
desorption behavior rather than adsorption. Therefore, to evaluate whether CO2
16
injection can be used for shale gas recovery, the result of desorption should be
17
investigated. The adsorption and desorption isotherms of mixture, CH4 and CO2 are
18
shown in Figure 8. From Figure 8 it can be seen that under the same condition of
19
pressure, the excess adsorption capacities of CO2 during desorption process is
20
evidently higher than that of CO2 during adsorption period. Meanwhile, the condition
21
of CH4 is just the reverse. In contrast with adsorption process, during desorption
22
period, when being mixed with CH4, the adsorption of CO2 is promoted with pressure 16
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decreasing, which is accordingly to say that during desorption process, CO2 present
2
advantage in competitive adsorption and more CH4 gas is replaced and desorbed. This
3
result indicates that CO2 has the potential to be used for enhancing CH4
4
Meanwhile, it also can be seen from Figure 8 that at the beginning of desorption
5
process, when the pressure just starts to decrease, the adsorption capacity of CO2
6
increases sharply to the maxim instead of decreasing. And then it decreases slowly as
7
pressure decreasing. For CH4 gas, the adsorption capacity decrease sharply almost as
8
soon as the pressure starts to decrease and then decreases slowly. During the pressure
9
decreasing period, CO2 shows preferential adsorption on shale samples, CH4 is
10
primarily to be desorbed due to preferential adsorption of CO2, thus when the pressure
11
begins to fall, the desorption rate of CH4 is relative higher and the excess adsorption
12
capacity decreases rapidly.
13
decreases gradually and the excess adsorption capacity decreases slowly.
As desorption process going on, desorption rate of CH4
14
When the pressure falling, because of that the adsorption energy of CH4 is lower,
15
CH4 is more easily to be desorbed from surface, which will provide vacant adsorption
16
sites. For CO2 gas, the decrease of pressure causes CO2 desorption, but at the
17
meantime, CO2 with higher adsorption ability will occupied part of the vacant
18
adsorption sites provided by CH4 desorption which results in the excess adsorption
19
capacity increasing. In terms of the result shown in Figure 8, it is investigated that the
20
adsorption amount of CO2 on vacant adsorption sites is larger than the desorption
21
amount due to pressure diminishing. At the beginning of desorption, due to the
22
relative higher desorption rate of CH4, lots of adsorption sites are available. Thus, at 17
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Energy & Fuels
1
this period, the excess adsorption capacity of CO2 rises quickly. As the process going
2
on, desorption rate of CH4 decreases as a result the increment of adsorption capacity
3
are not sufficient to offset the desorption capacity caused by pressure decreasing; at
4
the same time with pressure falling further, the desorption rate of CO2 rises. Therefore
5
at the later stage of desorption, desorption plays a dominant role and the excess
6
adsorption capacity of CO2 declines.
7 0.16
Adsorption (Mixture) Adsorption (CH4 of Mixture) Adsorption (CO2 of Mixture) Desorption (Mixture) Desorption (CH4 of Mixture) Desorption (CO2 of Mixture)
0.14
Excess Adsorption (mmol/g)
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60
Page 18 of 26
0.12 0.10 0.08 0.06 0.04 0.02 0.00 0
8
1000
2000
3000
4000
5000
Pressure (kPa)
9
Figure 8. Adsorption and desorption isotherms of Mixture, CH4 and CO2.
10
By comparing the desorption ratio of CH4 in pure component and mixture gas,
11
the feasibility of exploiting shale gas by CO2 injection is evaluated. Desorption ratio
12
(Dr) is defined as the proportion of CH4 desorption capacity and the total adsorption
13
capacity of CH4. According to Figure 3 and Figure 8, desorption capacity is calculated.
14
Meanwhile, desorption ratio per pressure drop (Dr’) was also calculated to reflect the
15
difficult level of exploring CH4. The result is shown in Table 4. It can be seen that Dr 18
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and Dr’ of mixture are both higher than these of pure CH4, it suggested that
2
desorption ratio of CH4 can be enhanced by 13.5% by the existence of CO2. This
3
result demonstrates that the utilization of CO2 for enhancing shale gas recovery has
4
certain theoretical feasibility.
5 6
Table 4. Comparison of desorption rate at unit pressure drop between pure
7
CH4 and mixture desorption experiments
Experiment
Starting
End
point
point
/kPa
8
Adsorption
Adsorption
capacity of
capacity of
Dr’ Dr/%
stating point/
end point /
(mmol/g)
(mmol/g)
(%/kPa)
/kPa
Pure CH4
4954.5
470.0
0.076
0.016
78.9
0.0178
Mixture
5038.5
546.1
0.081
0.006
92.6
0.0207
4. Conclusion
9
To evaluate the feasibility of the utilization of CO2 for enhancing shale gas
10
recovery, adsorption and desorption experiments of methane, carbon dioxide, and
11
mixtures of the two gases on shale have been operated and the adsorption and
12
desorption behaviors have been discussed. Based on the above experimental results,
13
the following conclusions can be draw.
14
(1) For the shale sample, the mesopore is dominant and the pore size is mainly
15
nanoscale. Meanwhile relative higher surface area can bring advantages for gas
16
sorption. 19
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1
(2) For pure CH4 and CO2, CO2 shows obvious advantage in adsorption.
2
However, shale has not exhibit preferential adsorption of CO2 for premixed gases.
3
Therefore the adsorption law of pure gas cannot be used to speculate the adsorption
4
behavior of premixed gas.
5
(3) For the mixture of CH4 and CO2, the different discipline of adsorption and
6
desorption process is presented. During adsorption process, CH4 is preferably
7
adsorbed; for desorption, CO2 shows higher adsorption ability on shale.
8
(4) The evaluation of shale gas recovery depends on desorption process rather
9
than adsorption process. In the desorption process, the existence of CO2 promotes
10
desorption of CH4, desorption ratio of CH4 was increased. Theoretically, CO2 can be
11
utilized for enhancing shale gas recovery.
12
AUTHOR INFORMATION
13
Corresponding Authors
14
*E-mail:
[email protected] (Z.Y.)
15
Notes
16
The authors declare no competing financial interest.
17
Acknowledgements
18
This work was supported by the National Natural Science Foundation of China
19
(51774302), National Key Technologies R&D Program of China (2017ZX05009-004),
20
the
21
(2462015QZDX01) and Sinopec (P15027).
Science
foundation
of
the
China
University
20
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of
Petroleum,
Beijing
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